№56/2021 Norwegian Journal of Development of the International
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№56/2021 Norwegian Journal of development of the International Science ISSN 3453-9875 VOL.1 It was established in November 2016 with support from the Norwegian Academy of Science. DESCRIPTION The Scientific journal “Norwegian Journal of development of the International Science” is issued 24 times a year and is a scientific publication on topical problems of science. Editor in chief – Karin Kristiansen (University of Oslo, Norway) The assistant of theeditor in chief – Olof Hansen • James Smith (University of Birmingham, UK) • Kristian Nilsen (University Centre in Svalbard, Norway) • Arne Jensen (Norwegian University of Science and Technology, Norway) • Sander Svein (University of Tromsø, Norway) • Lena Meyer (University of Gothenburg, Sweden) • Hans Rasmussen (University of Southern Denmark, Denmark) • Chantal Girard (ESC Rennes School of Business, France) • Ann Claes (University of Groningen, Netherlands) • Ingrid Karlsen (University of Oslo, Norway) • Terje Gruterson (Norwegian Institute of Public Health, Norway) • Sander Langfjord (University Hospital, Norway) • Fredrik Mardosas (Oslo and Akershus University College, Norway) • Emil Berger (Ministry of Agriculture and Food, Norway) • Sofie Olsen (BioFokus, Norway) • Rolf Ulrich Becker (University of Duisburg-Essen, Germany) • Lutz Jäncke (University of Zürich, Switzerland) • Elizabeth Davies (University of Glasgow, UK) • Chan Jiang(Peking University, China) and other independent experts 1000 copies Norwegian Journal of development of the International Science Iduns gate 4A, 0178, Oslo, Norway email: [email protected] site: http://www.njd-iscience.com CONTENT AGRICULTURAL SCIENCES Matsera O. THE EFFECT OF GROWING TECHNOLOGY ELEMENTS ON WINTER RAPESEED SEEDS AND QUALITY UNDER CONDITIONS OF RIGHT-BANK FOREST-STEPPE IN UKRAINE ...................................................................... 3 EARTH SCIENCES Bronnikova L. GEOMORPHOLOGICAL STRUCTURE OF SOIL COVER RELIEF OF THE VINNYTSIA REGION AS A FACTOR OF THE INTENSITY OF EROSION PROCESSES .................. 12 PHARMACEUTICS Nazarkina V., Popova I., Kurylenko Yu., Podkolzina M., Teterich N. ANALYSIS COMPETITIVENESS DRUGS OF THE NOOTROPIC GROUP ON PHARMACEUTICAL MARKET OF UKRAINE .............................................................. 21 PHILOSOPHICAL SCIENCES Khakimov N. SECOND HIGHER EDUCATION AS AN IMPORTANT FORM OF TRAINING COMPETITIVE STAFF IN UZBEKISTAN .............................................................. 26 TECHNICAL SCIENCES Vinogradova M., Аyzler P.P. Polyovyk V., Berezova G., OUTLOOK ON MASTERING OF COSMOS ................... 35 Deinychenko L., Koretska I. Gazizov M. RESEARCH OF THE PROCESS OF DESSERTS QUALITY TYPES OF USE OF VPN TUNNELS IN AN OPEN FORMATION .............................................................. 53 NETWORK .................................................................. 44 Tomchuk V. Maloshtan D., Kuzev I., WHY PLOUGHING REMAINS ACTUAL ........................ 61 Dragobetskyi V., Shlyk S., ShchetyninV. MATERIAL SAVING RESERVES IN SHEET STAMPING PRODUCTION ............................................................ 47 12 Norwegian Journal of development of the International Science No 56/2021 EARTH SCIENCES GEOMORPHOLOGICAL STRUCTURE OF SOIL COVER RELIEF OF THE VINNYTSIA REGION AS A FACTOR OF THE INTENSITY OF EROSION PROCESSES Bronnikova L. senior lecturer Vinnytsia National Agrarian University Abstract The results of studying the features of erosion resistance of soils of Vinnytsia region with regard to the fea- tures of geomorphological structure of the terrain (slope steepness) based on the results of recent surveys and outlined the main directions of reducing the intensity of erosion processes given the agro-technological features of the region. Keywords: soil, soil cover, water erosion, fertility, erosion processes. Introduction. Most of the territory of Vinnytsia are 250 to 350 m thick. The Cretaceous (Mesozoic) sed- region is located within the Ukrainian Crystal Shield iments are quite common in Transnistria. Like the Silu- which is part of the Eastern European platform. In the rian deposits, the Cretaceous rocks stretched in a wide north and northeast, the foundation of the shield rises strip along the Dniester, from the Zhvan and Karaets above the surface by 100-280 m above sea level. The rivers to the Kamyanka river basin. The thickness of the relief of the foundation is complicated by numerous lo- Cretaceous sediments reaches 40, sometimes 60 m. In cal tectonic uplifts and depressions, which are reflected comparison with the Paleozoic and Mesozoic sedi- in its current state. ments, Neogene sediments, in particular, the Sarmatian The foundation of the shield within the Vinnytsia and Baltic tiers, are widespread in a much larger part of region is composed of igneous and metamorphic crys- the region. talline rocks of the Archaea and Lower Proterozoic. On The purpose of the article. The eastern boundary top of the crystalline basement of the region there is a of the distribution of Sarmatian tier deposits passes ap- low-thickness sedimentary layer formed of Upper Pro- proximately through Vinnytsia, Humenne station, p. terozoic rocks and Cretaceous, Paleogene, Neogene Yurkivtsi (Nemyriv district), Dashiv village (Illinetsky and Quaternary systems of the Phanerozoic, on its district), Kuzmyntsi village (Haisynsky district), La- southwestern edge. The geological history of the region dyzhyn (Trostyanets district), Sobolivka (Haisynsky is complex. It also influenced the formation of relief [1, district), on the left bank of the Southern Bug to 2]. The foundation of the territory [3] consists of rocks, Haivoron (Kirovohrad region). Sarmatian sediments the formation of which dates back to Precambrian are represented mainly by oolite and shell limestones times. They are mainly granite gneisses. Outcrops of and have a thickness of 5 to 100 m. These sediments Precambrian rocks on the day surface take place in deep are well preserved in watersheds, and in river valleys ravines, gullies and in the form of rapids on rivers (es- they are blurred. Limestone deposits of the Sarmatian pecially on the Southern Bug and its tributaries and the Sea are widespread throughout Transnistria. Thus, in Dniester - near Yampol). Reddish and gray granites of the basin of the Rusava River, oolite limestones have a Precambrian origin occur in outcrops along the layer thickness of 80-85 m, and along the Kamyanets Markivka and Rusava rivers. Most outcrops of crystal- River - 25 m. lime. Deposits of the Baltic tier are mostly line rocks on the day surface are observed in the strip distributed in the left-bank part of the Southern Bug, in between the lines (conditionally) Kozyatyn-Pogreby- the central and southern parts of the region, mainly in shche and Mohyliv-Podilskyi-Yampil. Part of the watersheds. White loose sands, brittle sandstone, red, Ukrainian Crystal Shield, located within the Vinnytsia brown clays and pebbles alternate in the Baltic depos- region, has a general slope to the west-southwest. its. The thickness of the deposits is from 5 to 120 m (the Therefore, in the Dnieper, crystalline rocks are covered largest in the south-eastern part of the region). Anthro- with a thick layer of sedimentary sediments of Paleo- pogenic sediments are distributed throughout the re- zoic and Mesozoic age. gion. They are represented by brown clays, forest and Formulation of the problem. Silurian marine forest-like loams, alluvium on river terraces. In the sediments are quite common in the Dnieper. They are north-eastern part of the region, sand and pebble depos- represented by coarse-grained sandstones, green, gray its are very common, which are believed to have and purple shales, limestones. Silurian deposits are dis- brought here the melting glacial waters of the last gla- tributed in the area bounded (conditionally) by a line ciation (Dnieper). passing through the village of Zhvan (Murovano- Results. The relief of the territory is heterogene- Kurylovetsky district), Nemerchi station to the village ous, because in its formation a significant role was of Chernivtsi. Further to the southeast, the Silurian de- played by neotectonic movements of the earth's crust, posits are distributed in the lower reaches of the rivers climate and other factors and in the overall assessment Rusava and Yalanka, to the confluence of the Markivka in relation to sea level is elevated. and the Dniester. In some places, the Silurian sediments According to the scheme of geomorphological Norwegian Journal of development of the International Science No 56/2021 13 zoning, the territory of Vinnytsia region is located Podolsk Upland is inclined from north and north- within two geomorphological regions: Volyn-Podilska east to south and southwest, has a submeridional direc- and Pridnestrovsko-Pryazovska, in turn within these tion. This location, as well as the significant slope of two regions the following geomorphological subre- the surface in the southern direction determined the me- gions are distinguished: Podilska structural-denudation ridional and parallel tributaries of the Dniester River, upland, Baltic alluvial-delta plain, Pivna hydroglacial the valley of which is an essential element of the relief and hewn plain, West Dnieper denudation upland and of the Podolsk Upland. The second, no less important Central Dnieper denudation upland within two geomor- feature of the southern slopes of the elevation is a kind phological provinces - Podil and Dnieper. The Dnieper of asymmetry of its interfluves. The deep incision